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M Pahlow

Publications and source records attributed to M Pahlow.

3 recordsLinked to original sources

Model of the carbon concentrating mechanism in chloroplasts of eukaryotic algae.

A generic chloroplast-based model for the carbon concentrating mechanism (CCM) in eukaryotic algae is presented. The fine structure of chloroplasts is represented by separate compartments: marginal and bulk stroma, pyrenoid, girdle lamella, bulk thylakoids, and central lamella traversing the pyrenoid. The roles of the individual structural elements of the chloroplast with respect to the CCM and the effect of carbonic anhydrase activity in various compartments are analysed. Hypothetical HCO(-)(3)transport into the acidic thylakoid lumen is adjusted by imposing an optimization principle: a given [CO(2)] at the site of RuBisCO is achieved with minimum energy costs for the CCM. Our model is highly efficient in terms of saturation of RuBisCO carboxylase activity and the affinity of the chloroplast for CO(2), if either a girdle lamella or a pyrenoid is present. The highest efficiency is achieved with a pyrenoid. A eukaryotic CCM is not necessarily associated with accumulation of dissolved inorganic carbon (DIC) as in cyanobacteria. Chloroplasts are categorized into four types corresponding to morphological characteristics of all major algal classes with regard to the presence of pyrenoids, girdle lamellae, and the distribution of CA activity.

Carbon↗

Temporal trends in deep ocean Redfield ratios.

The Redfield ratio [carbon:nitrogen:phosphorus (C:N:P)] of particle flux to the deep ocean is a key factor in marine biogeochemical cycling. Changes in oceanic carbon sequestration have been linked to variations in the Redfield ratio on geological time scales, but this ratio generally is assumed to be constant with time in the modern ocean. However, deep-water Redfield ratios in the northern hemisphere show evidence for temporal trends over the past five decades. The North Atlantic Ocean exhibits a rising N:P ratio, which may be related to increased deposition of atmospheric nitrous oxides from anthropogenic N emissions. In the North Pacific Ocean, increasing C:N and C:P ratios are accompanied by rising remineralization rates, which suggests intensified export production. Stronger export of carbon in this region may be due to enhanced bioavailability of aeolian iron. These findings imply that the biological part of the marine carbon cycle currently is not in steady state.

Atlantic Ocean↗